4.7 Article

Impacts of Land Use/Land Cover Distributions on Permafrost Simulations on Tibetan Plateau

Journal

REMOTE SENSING
Volume 15, Issue 23, Pages -

Publisher

MDPI
DOI: 10.3390/rs15235586

Keywords

land use/land cover products; permafrost simulation; Tibetan Plateau; land surface model

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This study investigates the effect of land use and land cover uncertainty on permafrost simulation in the Tibetan Plateau. The results show that land cover has a greater impact on soil temperature simulations in regions with greater land use inconsistency. It is important to increase the model plant function types and carefully select land use and land cover products in order to improve the simulation performance of land-surface models in permafrost regions.
The Tibetan Plateau (TP) is distributed with large areas of permafrost, which have received increasing attention as the climate warms. Accurately modeling the extent of permafrost and permafrost changes is now an important challenge for climate change research and climate modeling in this region. Uncertainty in land use and land cover (LULC), which is important information characterizing surface conditions, directly affects the accuracy of the simulation of permafrost changes in land surface models. In order to investigate the effect of LULC uncertainty on permafrost simulation, we conducted simulation experiments on the TP using the Community Land Model, version 5 (CLM5) with five high-resolution LULC products in this study. Firstly, we evaluated the simulation results using shallow soil temperature data and deep borehole data at several sites. The results show that the model performs well in simulating shallow soil temperatures and deep soil temperature profiles. The effect of different land use products on the shallow soil temperature and deep soil temperature contours is not obvious due to the small differences in land use products at these sites. Although there is little difference in the simulating results of different land use products when compared to the permafrost distribution map, the differences are noticeable for the simulation of the active layer. Land cover had a greater impact on soil temperature simulations in regions with greater land use inconsistency, such as at the junction of bare soil and grassland in the northwestern part of the TP, as well as in the southeast region with complex topography. The main way in which this effect occurs is that land cover affects the net surface radiation, which in turn causes differences in soil temperature simulations. In addition, we discuss other factors affecting permafrost simulation results and point out that increasing the model plant function types as well as carefully selecting LULC products is one of the most important ways to improve the simulation performance of land-surface models in permafrost regions.

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